[vc_row css=”.vc_custom_1585241334448{padding-top: 80px !important;padding-bottom: 80px !important;}”][vc_column offset=”vc_col-lg-offset-0″][ultimate_heading main_heading=”RESEARCH” heading_tag=”h1″ main_heading_font_size=”desktop:40px;” main_heading_line_height=”desktop:50px;” sub_heading_line_height=”desktop:28px;”][/ultimate_heading][/vc_column][/vc_row][vc_row full_width=”stretch_row” bg_type=”bg_color” bg_color_value=”#eaeaea” css=”.vc_custom_1585250510433{padding-top: 50px !important;}”][vc_column][vc_row_inner][vc_column_inner][vc_column_text]In the context of global change, it is URGENT to generate and share reliable, representative and rigorous data and information that allows us to UNDERSTAND the natural processes that occur at different spatial and temporal scales to design and propose SUSTAINABLE solutions.
We have several lines of research in water and Earth sciences in different contexts (arid zones, Altiplano, forested temperate zones):[/vc_column_text][/vc_column_inner][/vc_row_inner][/vc_column][/vc_row][vc_row full_width=”stretch_row_content” bg_type=”bg_color” css=”.vc_custom_1585251337566{padding-top: 0px !important;padding-right: 50px !important;padding-bottom: 130px !important;padding-left: 50px !important;}” bg_color_value=”#eaeaea”][vc_column][vc_row_inner][vc_column_inner width=”1/5″]
[ultimate_heading main_heading=”HYDROGEOLOGY OF ARID AREAS” main_heading_font_size=”desktop:23px;” main_heading_line_height=”desktop:36px;” sub_heading_line_height=”desktop:28px;” sub_heading_margin=”margin-bottom:20px;” main_heading_margin=”margin-bottom:5px;”][/ultimate_heading][/vc_column_inner][vc_column_inner width=”1/5″][ultimate_heading main_heading=”ECOSYSTEMS AND GROUNDWATER” main_heading_font_size=”desktop:23px;” main_heading_line_height=”desktop:36px;” sub_heading_line_height=”desktop:28px;” sub_heading_margin=”margin-bottom:20px;” main_heading_margin=”margin-bottom:5px;”][/ultimate_heading][/vc_column_inner][vc_column_inner width=”1/5″][ultimate_heading main_heading=”HYDROLOGICAL MONITORING” main_heading_font_size=”desktop:23px;” main_heading_line_height=”desktop:36px;” sub_heading_line_height=”desktop:28px;” sub_heading_margin=”margin-bottom:20px;” main_heading_margin=”margin-bottom:5px;”][/ultimate_heading][/vc_column_inner][vc_column_inner width=”1/5″][ultimate_heading main_heading=”GEOLOGICAL AND HYDRAULIC HERITAGE” main_heading_font_size=”desktop:23px;” main_heading_line_height=”desktop:36px;” sub_heading_line_height=”desktop:28px;” sub_heading_margin=”margin-bottom:20px;” main_heading_margin=”margin-bottom:5px;”][/ultimate_heading][/vc_column_inner][vc_column_inner width=”1/5″][ultimate_heading main_heading=”INTEGRATION OF LOCAL KNOWLEDGE” main_heading_font_size=”desktop:23px;” main_heading_line_height=”desktop:36px;” sub_heading_line_height=”desktop:28px;” sub_heading_margin=”margin-bottom:20px;” main_heading_margin=”margin-bottom:5px;”][/ultimate_heading][/vc_column_inner][/vc_row_inner][/vc_column][/vc_row][vc_row full_width=”stretch_row” bg_type=”image” parallax_style=”vcpb-vz-jquery” bg_image_new=”id^2748|url^https://carpescience.com/wp-content/uploads/2019/06/Hidrogeologia_CS_1900.jpg|caption^null|alt^null|title^Hidrogeologia_CS_1900|description^null” bg_image_repeat=”no-repeat” bg_override=”ex-full” el_id=”aridareas” css=”.vc_custom_1585674082018{margin-top: 0px !important;padding-bottom: 50px !important;}”][vc_column][vc_row_inner css=”.vc_custom_1585270011190{margin-top: 60px !important;margin-bottom: 40px !important;}”][vc_column_inner]Water scarcity is the challenge of the 21st century. In 2016, 1.9 billion people were affected by water scarcity (27% of the world’s population). Estimates foresee that in 2050 there will be between 2.7 and 3.2 billion people affected. However, it is important to distinguish between physical and economic scarcity.
This map also distinguishes areas where water scarcity was not estimated (gray), because of lack of data. These areas also correspond to the arid and hyper-arid areas of the planet (in yellow) that represent 40% of the continents and 35% of the world population, of which 90% in developing countries.
The north of Chile is one of the driest areas on earth. Since the 1990s, the development of large mining projects has generated an increase in demography and water demand. Conflicts with native communities and farmers have been increasing. On the basis of what information are decisions made? What are the impacts of mining activities on water resources? How to reduce and mitigate this impact? What are the management strategies in such an environment, in the long term and with the communities as the main actor?
[/vc_column_text][/vc_column_inner][vc_column_inner width=”1/5″][vc_single_image image=”49683″ img_size=”full” alignment=”center” onclick=”link_image”][/vc_column_inner][/vc_row_inner][ult_tab_element tab_animation=”None” tab_title_color=”#ffffff” tab_background_color=”#008c8c” tab_hover_title_color=”#ffffff” tab_hover_background_color=”#f7941d” acttab_title=”#ffffff” acttab_background=”#f7941d” disp_icon=”Disables” resp_style=”Title”][single_tab title=”APPROACH AND PROJECT” tab_id=”1585257616658-2-2″][vc_row_inner content_placement=”top” css=”.vc_custom_1585323990420{margin-top: -12px !important;padding-right: 20px !important;padding-left: 20px !important;background-color: rgba(0,140,140,0.8) !important;*background-color: rgb(0,140,140) !important;}”][vc_column_inner][vc_column_text]
Our research focuses on the understanding and characterization of hydrological and hydrogeological processes in arid areas, with the aim of improving groundwater management in a context of increasing socioeconomic pressures and conflicts.
In particular, we seek to understand the groundwater recharge processes, through better identification of flows between hydrological compartments. We also seek to identify the impacts of the different anthropic activities on the availability of water resources, in particular the impact of mining activities in the head catchment.
[/vc_column_text][/vc_column_inner][/vc_row_inner][/single_tab][single_tab title=”Tamentica Environmental Project” tab_id=”1585257247763-10″][vc_row_inner content_placement=”top” css=”.vc_custom_1585324012443{margin-top: -12px !important;padding-right: 20px !important;padding-left: 20px !important;background-color: rgba(247,148,29,0.85) !important;*background-color: rgb(247,148,29) !important;}”][vc_column_inner width=”4/5″][vc_column_text]With theCorporación Norte Grande and the Aymara Community of Tamentica, located in the Quebrada de Guatacondo, Tarapacá Region, water resources in the catchment are being studied and monitored. In particular, we seek to characterize the hydrological and hydrogeological processes in the catchment, as well as the impact of two large mining projects located at the head of the basin on water resources. The monitoring and research work is carried out in a participatory and joint way with the community, integrating local knowledge into scientific knowledge.[/vc_column_text][/vc_column_inner][vc_column_inner width=”1/5″][vc_column_text]
Start Date: October 2016
ON-GOING
[/vc_column_text][/vc_column_inner][/vc_row_inner][/single_tab][single_tab title=”Characterization of groundwater recharge processes in arid and piedmont areas” tab_id=”1585257247914-1″][vc_row_inner content_placement=”top” css=”.vc_custom_1585324050605{margin-top: -12px !important;padding-right: 20px !important;padding-left: 20px !important;background-color: rgba(247,148,29,0.85) !important;*background-color: rgb(247,148,29) !important;}”][vc_column_inner width=”4/5″][vc_column_text]The Pica y Matilla Oasis, located in the Tarapacá Region in northern Chile, owes its oasis status to the presence of thermal springs (~ 32 ° C) and a shallow groundwater layer. The Pica aquifer has been the subject of studies since the 1960s, given its potential, in the middle of the desert, its possible connection with altiplanic basins and with the Pampa del Tamarugal aquifer, have motivated the studies since the 1960s. Today, the water table is decreasing and its water is salinized. Thanks to the study of the underground galleries of Pca and Matilla, we have characterized the different flows that feed the Pica aquifer and proposed a new conceptual hydrogeological model of the aquifer, which accounts for the mechanisms of recharge and discharge of the aquifer.[/vc_column_text][/vc_column_inner][vc_column_inner width=”1/5″][vc_column_text]
Start date: 2012
ON-GOING
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Understanding and characterizing these interactions between surface water, groundwater and ecosystems is key in the context of current climate change. It will allow to anticipate which are the ecosystems that will be most affected by climate change, and which will be more resilient. It will also allow to understand the role of ecosystems in groundwater storage, ensuring base flow in dry periods.[/vc_column_text][/vc_column][/vc_row][vc_row full_width=”stretch_row” bg_type=”bg_color” bg_color_value=”#e6e7e8″ el_id=”monitoring” css=”.vc_custom_1585674223913{padding-top: 80px !important;padding-bottom: 80px !important;}”][vc_column]
In arid and mountainous area, the temporal and spatial heterogeneity of the hydrometeorological variables and the complexity of the hydrological and hydrogeological processes require a more important amount of data, both spatially and temporally, to generate predictive hydrological and hydrogeological models. However, extreme weather conditions and access difficulty are a limitation to the production of data in these areas.
This is the case of northern Chile, one of the world driest areas and, nevertheless, with a population that is constantly increasing along with socioeconomic growth since the beginning of the large mining projects in the 1990s.
Since 2011, we work in the generation of meteorological and hydrological data in the Tarapacá Region, northern Chile. Particularly in the highest and most difficult areas, and where there are communities that need to understand the anthropic impacts that affect their ancestral way of life.
Through several tools (Installation of monitoring stations and sensors in remote areas, manual monitoring, participatory monitoring and use of local and ancestral knowledge), we managed to generate data on precipitation, flow, piezometric levels and water quality that allow us to characterize hydrological and hydrogeological processes in the catchment affected by climate change and large-scale mining activities.[/vc_column_text][/vc_column_inner][vc_column_inner width=”2/5″][dt_gallery_photos_masonry post_type=”posts” bwb_columns=”desktop:3|h_tablet:3|v_tablet:3|phone:3″ gap_between_posts=”4px” image_sizing=”resize” image_border_radius=”0px” project_icon_color=”#ffffff” project_icon_border_width=”0px” dis_posts_total=”9″ posts=”50950″ css_dt_gallery=”.vc_custom_1585670947330{margin-top: 30px !important;}”][/vc_column_inner][/vc_row_inner][/vc_column][/vc_row][vc_row full_width=”stretch_row” bg_type=”image” parallax_style=”vcpb-vz-jquery” bg_image_new=”id^50100|url^https://carpescience.com/wp-content/uploads/2020/02/DSC01566_1900-1.jpg|caption^null|alt^null|title^DSC01566_1900|description^null” bg_image_repeat=”no-repeat” bg_override=”ex-full” css=”.vc_custom_1585674198651{margin-top: 0px !important;padding-bottom: 50px !important;}” el_id=”heritage”][vc_column][vc_row_inner css=”.vc_custom_1585270011190{margin-top: 60px !important;margin-bottom: 40px !important;}”][vc_column_inner]
Rice field Kamchay Mear, Cambodia
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Water reserves in Aaqoura, Lebanon
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Rain water reserves, Palestine
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Water tank reserve, Yemen
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Water reserve, Wadi Mahmoud, Jordan
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Irrigation channels, Wadi Al-Nakhar, Oman
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Community meeting Kampong Cham Cambodia
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Air shaft qanat (lumbrera) in Pica, Chile
[/vc_column_text][/vc_column_inner][/vc_row_inner][/ultimate_carousel][/vc_column][/vc_row][vc_row css=”.vc_custom_1585661624997{padding-bottom: 60px !important;}”][vc_column][vc_column_text]The local and ancestral knowledge of native communities helps to address this lack of data. Those communities resort to a great diversity of indicators to predict the climate and adapt their activities, as a result of the millenary observation of nature. Although, in recent decades, rapid changes in the climate and its living environment, together with the arrival of new actors with productive interests in the watersheds where their territories are, have affected this prediction capacity and threaten their permanence. Based on a trust, local knowledge help to understand the processes that occur in the basin, to integrate local knowledge into scientific knowledge, in particular the hydrological and hydrogeological conceptual models. The participation of the communities is essential to identify areas of importance to monitor water resources, understand the history of flows, bring the scientific method to the territories and allow the communities themselves, with their continuous presence in the field, to collect information for the rest of the actors.[/vc_column_text][/vc_column][/vc_row][vc_row full_width=”stretch_row” bg_type=”bg_color” bg_color_value=”#e5e5e5″ css=”.vc_custom_1585661509959{padding-top: 60px !important;padding-bottom: 60px !important;}”][vc_column css=”.vc_custom_1585661579709{padding-right: 100px !important;padding-left: 100px !important;}”][vc_cta h2=”Do you want more information about these projects?” txt_align=”center” style=”custom” add_button=”bottom” btn_title=”Write to us!” btn_color=”warning” btn_align=”center” btn_link=”url:https%3A%2F%2Fcarpescience.com%2Fen%2Fcontact%2F|title:Contact||” custom_background=”#ffffff” custom_text=”#008c8c”][/vc_cta][/vc_column][/vc_row]






